• 한국해양학회지
• /
• 제30권4호
• /
• pp.341-354
• /
• 1995

동해의 8개 정점에서 해수 및 추출된 용존 유기물의 형광특성과 아미노산 조성이 연구되었다. C-18 Sep-Pak cartridge에 의해 추출된 시료는 3차원 형광특성 분석에 따 라 생거대물질과 지구거대물질로 구분되었다. 전 조사 정점을 통하여 생거대물질(ex : 280 nm/em : 330 nm)은 표층이 높고 수온약층 아래에서 점차 감소하는 것으로 나타났 으며 이는 표층혼합층의 생물 활동에서 기인된 분해가능한 생거대물질이 수온약층 부 근 및 저층에서 활발한 미생물 분해과정에 의해 감소하는 것으로 사료된다. 한편 이와 는 역상관계를 보이는 지구거대물질 (ex : 330 nm/em : 430 nm)은 표층은 낮고 수온약 층 아래에서 증가하였는데 이는 표층에서 생성된 생거대물질 및 입자유기체가 생물 분 해 후 재축합 과정을 거쳐 난분해성의 지구거대물질로 전환된 것으로 사료된다. HPLC 를 이용하여 해수와 추출된 유존유기물의 아미노산 조성을 분석하였다. 분석결과 Glycine, serine 그리고 alanine등이 우점하였으며, 전체 농도의 50% 이상을 차지하는 것으로 조사되었다. 해수중의 용존 자유아미노산 농도는 표층이 0.7∼1.8um 범위로 저 층 0.2∼0.4um보다 높게 측정되었다. 추출된 유기물중 alanine의 D/L racemice ratio 측정결과 저층보다 표층이 상대적으로 낮은 값을 보였으며 이는 표층의 생거대물질이 연령이 젊고 재순환이 빠르며 생물 분해가능성이 큰 물질임을 시사하고 있다.

• 대한수의학회지
• /
• 제27권2호
• /
• pp.259-267
• /
• 1987

Enterotoxigenic E. coli (ETEC) cause an acute diarrhea (white scour) in both animals and humans. The disease process initially involves the adherence and colonization of the mucosal surface of the small intestine, followed by the elaboration of a heat-labile enterotoxin (LT) and/or heat-stable enterotoxin (ST). Intestinal adherence or colonization by ETEC is generally mediated by a specific surface-associated pilus (fimbrial) antigen that endows the bacteria with the capacity to adhere to epitherial cell surface. Fourteen monoclonal antibodies (MAbs) directed against pili antigens of ETEC were obtained by cell fusion/hybridoma technique. They were characterized by indirect immunofluorescence assay (IFA), and divided into four groups: specific to K99 antigen (group 1), cross-reactive with K99 and F41 antigens (group 2), specific to K88 antigen (group 3) and specific to 987P and K88 antigens (group 4), respectively. These MAbs demonstrated the distinct pili (K) antigens on the surface of ETEC by IFA, and could be utilized as diagnostic reagent for the identification of ETEC. When eighty-seven field isolates of E. coli from piglet with diarrhea were tested by group 3 MAb, fourty-two strains (48.3%) has K88 pilus antigen suggesting that this is one of the major pilus antigen of ETEC present in fifeld.

• 한국환경과학회지
• /
• 제6권6호
• /
• pp.595-604
• /
• 1997

To investigate characteristics of biogeochemical environment of the Korea Deep Ocean Study(KODOSI area in the northeast Pacific Ocean, we preferentially measured Inorganic nutrients and fluorescent organic matters. Typically. the permanent thermocline was well developed at the depth of 200~1000m In the study area. Nitrate. phosphate and silicate were low In the surface mixed layer and Increased with depth. N/P and N/Si showed 15 and 0.2 respectively In the deeper layer. Two fluorophores, biomacromolecule(protein-like) and geomacromolecule (humid-like) , were observed by three dimensional fluorescence excltatlon/ emission spectra matrix. Biomacromolecule(maximum fluorescence at $Ex_{280m}/Em_{330nm}$) ranged from 41.9 to 147.0 TU with its maximum In the surface mixed layer and minimum in deeper water, This is a same trend that has been reported for DOC in the equatorial Pacific. This suggests that biomacromolecule might be labile and converted to refractory humic substance after bacterial degradation In the deeper layer. On the contrary, geomacromolecule(maximum fluorescence at $Ex_{330m}/Em_{430m}$), ranged from 7.6 to 46.5 QSU, showed minimum in the surface nixed layer(euphotic zone) Implying photodegradation and then increased with depth at all stations. In the characteristics of vertical profiles, the relationship between biomacromolecule and geomacromolecule showed negative correlation. Such trend can be attributed to biochemical regeneration or formation of fluorescent materials accompanying oxidation and rennnerallzation of settling organic matter.

• Journal of the korean society of oceanography
• /
• 제35권1호
• /
• pp.16-33
• /
• 2000

In order to measure the vertical fluxes of particles and reactive radionuclides such as thorium and polonium isotopes, Dunbar-type sediment traps were freely deployed at the Ulleung Basin and in warm and cold water masses around the polar front of the East Sea. We estimated the ratios of the catched (F) to the predicted $^234$Th fluxes (P) using natural tracers pair $^234$Th-$^238$U. The F/P ratios are decreased with increasing water depth. Whereas the concentrations of suspended particles are homogeneous in water column, the mass fluxes are also decreased with increasing water depth like the F/P ratios. These facts indicate that organic matters of settling particles are destructed within the euphotic layer due to decomposition. Whereas regenerations of sinking particles are negligible in the cold water mass, about 80% of them are regenerated in the warm water mass during falling of large particles. These downward mass fluxes are closely correlated with their primary productions in euphotic zone. The activities of $^234$Th, $^228$Th and $^210$Po in the sinking material were increased with water depth. Because $^234$Th steadily produced in the water column are cumulatively adsorbed on the surface of sinking particles, vertical $^234$Th fluxes were observed to increase with water depth. Therefore, these sinking particles play important roles in transporting the particle reactive elements like thorium from surface to the deep sea. The scavenging processes including adsorption and settling reactions generate radio-disequilibrium between daughter and parent nuclides in water column. The activity ratios of $^234$Th/$^238$U and $^228$Th/$^228$Ra were observed to be < 1.0 in the surface water and approached to be equilibrium below the thermocline. The extent of the deficiency of daughter nuclides compared to the parents nuclide was highly correlated with the vertical particle flux. Because most of the $^210$Po in the surface water are scavenged on a labile phase and are recycled at sub-surface depths (< 200 m), the $^210$Po are always observed to be excess activities compared to $^226$Ra in surface water.

• Bulletin of the Korean Chemical Society
• /
• 제28권12호
• /
• pp.2481-2485
• /
• 2007

Spatially resolved, quantitative, non-destructive analysis using synchrotron x-ray reflectivity (XR) with subnano-scale resolution was successfully performed on the nanoporous organosilicate thin films for low dielectric applications. The structural information of porous thin films, which were prepared with polymethylsilsesquioxane and thermally labile 4-armed, star-shaped poly(ε-caprolactone) (PCL) composites, were characterized in terms of the laterally averaged electron density profile along with a film thickness as well as a total thickness. The thermal process used in this work caused to efficiently undergo sacrificial thermal degradation, generating closed nanopores in the film. The resultant nanoporous films became homogeneous, well-defined structure with a thin skin layer and low surface roughness. The average electron density of the calcined film reduced with increase of the initial porogen loading, and finally leaded to corresponding porosity ranged from 0 to 22.8% over the porogen loading range of 0-30 wt%. In addition to XR analysis, the surface and the inner structures of films are investigated and discussed with atomic force and scanning electron microscopy images.

• 환경위생공학
• /
• 제12권3호
• /
• pp.31-39
• /
• 1997

The seasonal and spatial changes in dissolved organic carbon(DOC) in Lake Kasumigaura, a shallow and eutrophic lake, were analyzed from October 1992 to October 1995. The proportion of T-DOC was classified by labile(L-DOC) and refractory DOC(R-DOC) on the basis of long-term incubation, fractionated the molecular weight of T-DOC by ultrafiltration. The porewater DOC were measured at sedimental surface of the central basin in order to evaluate the DOC released from the sediment. The proportion of L-DOC and R-DOC were accounted for about 15% and 85% of T-DOC in the central basin, respectively. The molecular weight(MW) distribution occupied some 60% of the low and medium MW. The horizontal variation of T-DOC concentrations trended to higher in the central basin than in the inlet of influent rivers, because of contribution by autochthonous organic carbon loading. The seasonal variation of T-DOC showed to higher summer than winter in the inlet of influent, but at the central basin it fluctuated little seasonally. During the high increase of porewater DOC in 1994 evaluated the high release possibility from the sediment surface (10cm). The present study suggests that autochthonous organic carbon loading must be controlled for improving the water quality of the eutrophic lakes.

• 공업화학
• /
• 제30권5호
• /
• pp.620-626
• /
• 2019

본 연구에서는 $Cu/CeO_2$ 촉매의 함량과 소성온도를 제어함으로써 촉매의 구조적 특성이 CO 산화반응에 미치는 영향과, $100{\sim}300^{\circ}C$의 온도범위에서 촉매의 CO 전환율을 평가하였다. 촉매의 구조적 특성이 변화함에 따라 촉매의 화학적 특성에 미친 영향을 확인하기 위해 XRD, Raman, BET, $H_2-TPR$, XPS 분석을 수행하였다. 이때, Cu와 Ce의 치환 결합이 형성되는 것을 확인하였고, Cu를 5 wt.% 담지한 촉매를 $400^{\circ}C$로 소성하였을 때 Cu와 Ce의 결합을 많이 이루고 있는 것으로 판단하였다. Cu와 Ce의 결합은 Raman 분석 상에서 peak의 이동과, $H_2-TPR$에서 나타난 peak를 통해 확인하였다. 또한 산화상태 분석을 통하여 치환 결합을 쉽게 이룰 수 있다고 알려져 있는 $Ce^{3+}$종과 반응에 더욱 쉽게 기인할 수 있는 표면 산소종(surface labile oxygen)이 많이 형성되어 있는 것을 확인하였다. 이때, 본 연구에서 사용한 촉매의 CO 전환율은 $150^{\circ}C$에서 100%에 가까운 수치를 나타내는 것을 확인하였다.

• 한국토양비료학회지
• /
• 제49권6호
• /
• pp.669-676
• /
• 2016

A field study was conducted to determine the runoff loss of N and P in small scale of red pepper field plots (10% slope), consisting of three different plots with black polyethylene vinyl mulching (mulching), ridge without mulching (ridge), and flat without ridge and mulching (flat). Composted manure and urea as a basal application were applied at rates of $20MT\;ha^{-1}$ and $93kg\;N\;ha^{-1}$, respectively. Urea at $189kg\;N\;ha^{-1}$ and fused phosphate at $67kg\;P_2O_5\;ha^{-1}$ were additionally applied on June 25 with different fertilization methods, broadcast application in flat plot and hole injection in ridge and mulching plots. Plant uptake of N and P was positively correlated with their respective concentrations in surface soil: mulching > ridge > flat plots. The runoff loss by soil erosion was higher in flat plot than ridge and mulching plot with contour line. Nitrate loss by the runoff water had no significant differences among three surface management practices, but the higher average value in ridge and mulching plots than flat plot. Especially, the flat plot had no phosphate loss during summer season. This is probably due to low labile P content in surface soil of flat plot. In the summation of soil and water loss, flat plot was higher in N and P loss than ridge and mulching plot with contour line. Nevertheless, the nitrate and phosphate loss by runoff water could be more important for non-point source management because the water could meet the river easier than eroded soil because of re-deposition around slope land.

• 한국지반환경공학회 논문집
• /
• 제13권4호
• /
• pp.53-59
• /
• 2012

본 연구에서는 지오폴리머계 그라우트재(HIT)의 강도 및 내구성 특성을 분석하기 위하여 일축압축강도시험, SEM, 공시체 표면변화관찰 및 용탈시험을 실시하였다. 일축압축강도시험 결과, HIT의 경우 초기강도가 높고, 재령일이 경과할수록 강도가 증가하는 경향을 보였으나, SGR과 LW 경우 재령 28일 이후 강도가 감소하는 경향을 보였다. 이는 SEM 결과와 일치하였으며, HIT의 경우 지속적인 수화반응을 통하여 밀실한 형태의 C-S-H 수화물이 다수 분포함을 확인할 수 있어 물유리계 재료보다 강도 및 내구성이 우수한 칼슘실리케이트 수화물을 형성함을 알 수 있었다. 또한 공시체의 표면변화 및 용탈시험 결과에서도 양생 6개월이 지난 시점에서 HIT의 경우 양호한 표면을 유지했으며 중량감소율도 극히 미미했다. LW, SGR의 경우에는 표면의 수축정도가 심했으며, 중량감소율도 HIT보다 큰 것으로 나타나 내구성이 떨어지는 것으로 나타났다. 종합적으로 HIT가 물유리계 재료보다 강도, 내구성면에서 우수한 특성을 나타내는 것으로 나타나 해상구조물 그라우트재로 적합할 것으로 판단된다.

• Journal of the korean society of oceanography
• /
• 제36권3호
• /
• pp.59-71
• /
• 2001

In order to investigate the temporal variability of dissolved and particulate trace metals in the Han River, water samples were collected intermittently at two sites for 3 years (August 91 to December 94). Surface seawaters covering the range of salinity were also collected at the estuarine region to evaluate the role of estuary for the riverine fluxes of trace metals within the estuary during October 95 and 96. During the study period, dissolved metal concentrations in riverwaters varied by a factor of 5-10 for Fe, Ni, Co and Cu and 50-100 for Mn, Cd and Pb depending upon the water level; high concentration during the low water and low concentration in high water period except for Fe. The concentration of dissolved Fe increased with increasing water discharge. These concentration-discharge relationships of the studied trace metals are explained by the successive dilution of waters from two different origins, which can be presumably identified as anthropogenic discharges and watershed flushing. Although estuarine waters at early mixing region were not collected due to the difficulty of sampling, mixing behaviors of metals were inferred from the concentration-salinity relationships through the laboratory mixing experiment and field sampling, and distribution coefficients between dissolved and labile particulate phases. It is suggested that the Han River estuary plays a role of accumulating Fe, Mn, Co and Pb from riverine sources due to high turbidity caused by strong tidal current, whereas this system serves as a source of dissolved Cd due to release caused by extended residence time of riverine particles.